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Rum

The mountainous, rugged island of Rum is the eroded remains of an early Tertiary volcanic centre that existed at the time of the opening of the North Atlantic Ocean. Many of the rocks found on Rum consist of layered ultramafic rocks - remnants of the base of the volcano's magma chamber. It is not the only volcanic centre on the west coast of Scotland to exhibit such layering, but the examples seen on Rum are well exposed and in an excellent state of preservation. They have become internationally important in their contribution to the understanding of the origins of layering igneous intrusions. As with the other Scottish Tertiary volcanic centres, Rum has been studied by many esteemed geologists such as John Macculloch (1773 - 1835), John Wesley Judd (1879 - 1914) and Sir Archibald Geikie, before being followed by more recent researchers such as Dr Alfred Harker (1859 - 1939) and Sir Edward Bailey (1881 - 1965).

Askival and Hallival

Askival and Hallival mountains of the Rum Cuillin.
Image provided by Scottish Natural Heritage

The Rum Complex was intruded into Lewisian basement, Torridonian sandstones (Precambrian), Mesozoic sedimentary rocks and early Tertiary lavas. The complex itself evolved in two main stages. Initially, intrusive and extrusive activity was charged by acid magmatism and associated with ring-faulting. It is thought that the complex underwent repeated doming and subsidence (within the cauldron) at this time. Rocks associated with this first phase include porphyritic felsite, volcanic breccias and tuffs.

mountains of the Rum Cuillin

Askival and Hallival mountains of the Rum Cuillin.
Image provided by Scottish Natural Heritage

The layered ultrabasic rocks were intruded during the second stage. The parent magma is considered to be either high-temperature picritic basalt or feldspathic peridotite that was subject to the right conditions that enabled it to rise to within a short distance of the Earth's surface before crystallising. The intrusions consist of sixteen layers of alternating feldspathic peridotite, troctolite, troctolitic gabbro, feldspathic gabbro and anorthosite.

Note: The Rum volcanic centre forms part of the North Atlantic Tertiary Igneous Province, along with the other centres of Skye, Arran, Ardnamurchan, Mull and St. Kilda.

Further reading:

Craig, G.Y. 1991. Geology of Scotland. 3rd edn. The Geological Society, London.

Emeleus, C.H. & Gyopari, M.C. 1992. British Tertiary Volcanic Province, Geological Conservation Review, Series No. 4. Joint Nature Conservation Committee, Peterborough.

RUM NNR Website

 

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